在中国西南部的黑龙江湖中发现的300年气候变化和潜在的人类遗传证据
Jianing Fan1, Yongbo Wang1, Kai Cui1
1College of Resource Environment and Tourism, Capital Normal University, 100048 Beijing, PR China.
The Science of the total environment
|December 6, 2023
概括
黑龙江湖的沉积物记录显示,气候在三百年内发生了变化. 1910年以后,人类活动对该地区的影响越来越大,这表明中国西南部的人类世过渡.
科学领域:
- 古气候学 古气候学
- 环境科学 环境科学
- 地质地质地质地质地质地
背景情况:
- 人类世概念强调人类对地球系统的影响.
- 高分辨率记录对于理解区域变化至关重要.
- 中国西南的恒达山脉对环境变化非常敏感.
研究的目的:
- 为了重建过去的气候和环境变化在黑龙江湖在过去的三个世纪.
- 研究自然和人为因素对沉积的影响.
- 为了确定中国西南部人类纪的潜在证据.
主要方法:
- 从黑龙江湖收集了一个连续的沉积物核心.
- 分析了高分辨率的沉积物代理物:颗粒大小,地质化学和有机物质含量.
- 将沉积物数据与区域古气候记录和历史人类活动数据进行比较.
主要成果:
- 在温暖,潮湿的条件下 (1717-1800年),湖泊水位较高,随后湿度下降.
- 太阳活动影响了区域气候,但1910年后的代理因素偏离了自然气候趋势.
- 公元1950年以后的人类活动增加可能改变了侵蚀和沉积,与自然气候变化脱.
结论:
- 黑龙江湖的沉历史显示,在过去的三个世纪里,从自然流程向人类主导的流程过渡.
- 由人口扩张驱动的人类活动的加剧是最近环境变化的一个关键因素.
- 这些发现提供了中国西南部人类纪的潜在证据.
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